Seismic heterogeneous structure in the lowermost mantle beneath the southwestern Pacific

The P and S wave velocity structure of the D″ layer beneath the southwestern Pacific was investigated by using short‐period data from 12 deep events in the Tonga‐Fiji region recorded by the J‐Array and the Hi‐net (two large‐aperture seismic arrays) in Japan. Reflected wave beam forming (RWB) and a m...

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Veröffentlicht in:Journal of Geophysical Research. B. Solid Earth 2004-09, Vol.109 (B9), p.B09304.1-n/a
Hauptverfasser: Kito, Tadashi, Krüger, Frank, Negishi, Hiroaki
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Sprache:eng
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